Xref: utzoo sci.bio:4059 sci.aquaria:988 sci.environment:8852 Path: utzoo!censor!geac!torsqnt!news-server.csri.toronto.edu!cs.utexas.edu!sun-barr!lll-winken!unixhub!shelby!rosentha@sierra From: rosentha@sierra.STANFORD.EDU (rosentha) Newsgroups: sci.bio,sci.aquaria,sci.environment Subject: Re: coral reefs, C02, food, and farming. Message-ID: <18@sierra.STANFORD.EDU> Date: 3 Dec 90 21:44:35 GMT References: <720@sierra.stanford.edu> <90337.112001JAHAYES@MIAMIU.BITNET> Organization: Stanford University Lines: 23 J Hayes had a point that calcium might be the limiting factor in C02 fixation, and that C02 is released when Calcium carbonate is precipitated. This is true but a little misleading. Calcium Bicarbonate has two bicarbonate ions. When a reaction removes a C02 from the disolved HC03- then usually a molecule of CaC03 precipitates out. This is probably the reaction that coral uses to build its skeleton. I would like to know how much of the corals photosynthesis goes into reef building and how much goes into respiration. This reef building activity seems quite similar to what the freshwater gardeners call biogenic decalcification, where plants absorb bicarbonates from the water rather than dissolved C02, and precipitate calcium carbonate all over the place. This is not usually a good situatin in a plant tank, and indicates too much light for the available C02. How slowly do reefs really grow? If a one square kilometer area grew a 1 cm layer of Calcium carbonate per year, then we would be fixing 10^10 cc's of carbonate each year. This probably weighs on the order of 10^7 kilograms or 20 million pounds. This is not that small a number is it? PEter Rosenthal Brought to you by Super Global Mega Corp .com